Intermediate Lakes of the Chulym and Kargat River Valleys and Their Role in the Evolution of the Lake Chany Basin | Sciact - CRIS-system of Boreskov Institute of Catalysis

Intermediate Lakes of the Chulym and Kargat River Valleys and Their Role in the Evolution of the Lake Chany Basin Full article

Journal

Russian Geology and Geophysics
ISSN: 1068-7971

Output data

Year: 2018, Volume: 59, Number: 5, Pages: 541-555 Pages count : 15 DOI: 10.1016/j.rgg.2018.04.007

Tags

paleolimnology; paleohydrology; lakes; Holocene; West Siberia; basin of Lake Chany

Authors

Krivonogov S.K. ^1,2 , Gusev V.A. ^1,2 , Parkhomchuk E.V. ^2,3 , Zhilich S.V. ^1,4

Affiliations

1	V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2	Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia
3	G.K. Boreskov Institute of Catalysis, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Lavrent’eva 5, Novosibirsk, 630090, Russia
4	Institute of Archeology and Ethnography, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Lavrent’eva 17, Novosibirsk, 630090, Russia

Funding (4)

1	Russian Foundation for Basic Research	15-05-00678 (115013010277)
2	Russian Foundation for Basic Research	16-05-00369 (АААА-А16-116020110168-1)
3	Russian Foundation for Basic Research	17-45-540527 (АААА-А17-117062710048-9)
4	The Ministry of Education and Science of the Russian Federation	14.Y26.31.0018 (АААА-А17-117051050004-4)

The Chulym and Kargat Rivers flow through chains of saucer-shaped depressions, which are swampy meadows or drainage lakes. In the past, all of them were lakes short-lived in different Holocene periods. These depressions accumulated a significant amount of the Chulym and Kargat runoff and thus influenced the water balance of Lake Chany. Our studies have reconstructed the history of these depressions. A model describing their filling with sediments is proposed. The lacustrine sediments penetrated by boreholes and pits are dated by the radiocarbon method at 6.3-2.0 cal. kyr BP. The data obtained explane the long existence of Lake Chany as a shallow basin and rise in its level at ~ 2 kyr BP.

Krivonogov S.K. , Gusev V.A. , Parkhomchuk E.V. , Zhilich S.V.
Intermediate Lakes of the Chulym and Kargat River Valleys and Their Role in the Evolution of the Lake Chany Basin
Russian Geology and Geophysics. 2018. V.59. N5. P.541-555. DOI: 10.1016/j.rgg.2018.04.007 WOS Scopus РИНЦ OpenAlex

Кривоногов С.К. , Гусев В.А. , Пархомчук Е.В. , Жилич С.В.
Промежуточные озера долин рек Чулым и Каргат и их роль в эволюции бассейна озера Чаны
Геология и геофизика. 2018. Т.59. №5. С.673-689. DOI: 10.15372/gig20180507RSCI РИНЦ OpenAlex

Submitted:	Feb 16, 2017
Accepted:	Sep 20, 2017
Published print:	May 1, 2018
Published online:	May 3, 2018

Web of science:	WOS:000432475000007
Scopus:	2-s2.0-85046633606
Elibrary:	35520811
OpenAlex:	W2801602227

DB	Citing
Web of science	7
Scopus	8
Elibrary	9
OpenAlex	9